-the presence of plastic zone where lava originates
Core
- about 3500 km thick
-it is divided into outer and inner core
-composed of iron and nickel
- hottest layer with a temp of 6,000 C to 10,000 C
Outer core- liquid; 2,300 km thick
Inner core- solid; 1,200 km thick
· Continental Drift Theory- in 1912, Alfred Wegener, a German geophysicist. Supercontinent is refered as “Pangea” (meaning all land). States that forces on Earth’s crust caused it to break into separate crustal plates and it looks like a jigsaw puzzle
Plate Tectonic Theory- lithosphere is made up of several individual plates of different sized. It states that plates that carry continental and oceanic crusts are in constant motion
Fold- when a rock is subjected to compressive stress, it begins to buckle and fold
FoldedMountains- folding occurs when great pressure and high temperature push the horizontal layer of rocks. As a result, the anticline forms mountains and hills, the syncline forms valleys
Crest or Anticline- elevated portion of the fold
Syncline or Through- lower portion of the fold
Faults- are fractures on rocks along which movement has occurred. It is the slippage of rock layers along the crack. Happens if one part moves relative to the other part, the fracture is called a fault
Block Mountains- when faulting occurs over a wide area on Earth’s surface
Earthquake- shaking of the ground. It happens when the crustal plate moves
Seismograph- an instrument that measures the motion of the ground during earthquakes
Seismograph- an instrument that can detect earthquakes.
Seismologists- experts on earthquakes
Seismogram- tracing earthquake motion
Types of Earthquakes
· Volcanic Earthquake- shaking off the ground. It happens in a strong volcanic eruption
· Tectonic Earthquake- caused by movement of Earth’s crust or crustal plate or faulting
NOTE: Tectonic Earthquake may occur above the ground or beneath the ocean
Richter Scale- an instrument we use in measuring the earthquake’s magnitude. It was made by Charles F. Richter, he is an American seismologist.
Magnitude- refers to the amount of energy released by an earthquake, from its focus. It uses numbers with decimals
Intensity- refers to the effect of an earthquake, especially the damage. Uses roman numerals
Mercalli Scale or Rossi-Forel Scale- an instrument used in measuring the intensity of an earthquake
Focus- break in the ground caused by the pressure of the moving rocks. This is where the earthquake originates
Epicenter- ground above the focus. Starting point of Earth’s surface of an earthquake
Philippine Institute of Volcanology and Seismology (PHILVOCS)- government agency concerned with earthquakes and volcanic eruptions in the Philippines
Circumpacific Ring of Fire or Pacific Ring of Fire- it is a 2500-mile chain of volcanoes and seismically active sites of Earthquakes and volcanic eruptions. It is also an area where crustal plates are weak
Volcano- opening in the Earth’s crust where lava, molten rocks, and gaseous materials are forced out through the opening
Vent- an opening, as in a wall, serving as an outlet for air, smoke, and fumes
Crater- the cone-shaped mountain with a funnel-shaped opening
Lava Flow- a stream or sheet of molten or solidified lava
Sill- an intrusive body of magma that pushes its way between layers of sediment
Ash Cloud- a cloud of gas, steam, ash, dust, and coarser fragments that form during an explosive volcanic eruption and commonly gets blown long distances
Secondary Vent- a vent or tube that connects to the secondary cone for the lava to flow
Throat- entrance of a volcano. The part of a conduit that ejects lava and volcanic ash
Conduit- an underground passage where magma travels through
Magma Chamber- a reservoir of magma in the Earth’s crust where the magma may reside temporarily on its way from the upper mantle to the Earth’s surface
Explosive Volcanic Eruption- large amounts of pyroclastic materials are ejected by the volcano into the air. It occurs when gasses in magma are trapped, causing a build-up of pressure in the magma chamber
Pyroclastic Materials- contains lava, ashes, volcanic gases, and rocks
Non-Explosive Eruption- lava just flows out of the crater and the gaps of the volcano. This kind of eruption happens when there is less pressure in the magma chamber
Kinds of Stages of Volcano
· Active Volcano- currently erupting or showing regular signs of activity like earthquakes, and significant gas emission
· Dormant Volcano- erupted and then entered a long period of inactivity. It is also called as “Sleeping Volcano”